The Critical Reception of Beethoven’s Compositions by His German Contemporaries, volume 2

The volumes in The Critical Reception of Beethoven's Compositions by His German Contemporaries bring to light contemporary perceptions of Beethoven's music, including matters such as audience, setting, facilities, orchestra, instruments, and performers as well as the relationship of Beethoven's music to theoretical and critical ideas of the eighteenth and nineteenth centuries. These documents, most of which appear in English for the first time, have been compiled from German-language periodicals published between 1783 and 1830. They present a wide spectrum of insights into the perceptions that Beethoven's contemporaries had of his monumental music. This is the second in a projected four-volume series. It begins with Opus 55, the Eroica, and ends with Opus 72, Fidelio.

Diatoms and Tonsteins as Paleoenvironrnental and Paleodepositional Indicators in a Miocene Coal Bed, Costa Rica

Fresh-water diatoms are present in coal, and tonsteins (altered volcanic ash) are interbedded with the coal, in the Miocene Venado Formation on the southwest margin of the Limon Basin, in Provincia Alajuela, northern Costa Rica. The Venado Formation is composed of more than 300 m of mudstone, siltstone, sandstone, limestone, volcaniclastics, and coal beds. The coal beds are of unknown lateral extent and mainly occur in the middle part of the formation. The Pataste coal bed occurs near the middle of the formation and is divided into three parts by two tonstein layers. The abundance of biogenic opaline material (diatoms) in the coal is believed to be a direct response to an influx of silica from volcanic tuffs that Later altered to the tonsteins. Diatoms are a useful microscopic tool for identifying the depositional environments of the Pataste coal deposit. The diatoms identified include Aulacosira ambigua, Pinnularia sp., Eunotia spp., and Achnanthes exigua, among others. The abundance of Aulacosira arnbigua suggests that an open-water lacustrine environment was present locally. Achnanthes exigua and the remaining diatom species are benthic forms that lived in shallow fresh-water to slightly acidic swamp environments. The different types of diatoms found in the coal indicate that swamp environments were intermixed with lacustrine environments during the formation of the peat deposit or that the coal records environmental changes through time.